GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    Publication Date: 2020-10-28
    Description: Petrological and geochemical data of the Upper Cretaceous volcanic rocks from Western Sicily are here reported with the aim to provide new information about the African paleomargin magmatic activity before the onset of the Alpine Orogeny. The studied alkaline basalts and basanites/nephelinites crop out as pillow breccias interbedded within the carbonate platform sequence of the Capo San Vito Peninsula. Abundances and ratios of incompatible elements resemble OIB-type volcanics from intraplate environment. They were generated from a low partial melting degree of a mantle source located in the transition zone between garnet- and spinel-lherzolite fields. Comparison with literature data of the coeval Hyblean volcanics show similar geochemical features of a plausible common source for the anorogenic magmas involved in their genesis. The Cretaceous magmatism of the S. Vito Lo Capo Peninsula is the result of magmatic intrusions in response to the extensional tectonic regime of the African plate northern edge.
    Description: Published
    Description: 19-35
    Description: 2TR. Ricostruzione e modellazione della struttura crostale
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2021-01-21
    Description: The ―Marmi Mischi‖ (mixed glass mosaic tesserae) are artificial calcium-rich glass decorations, typically used in southern Italy and Sicily during the Baroque period (1600-1700) to decorate walls and altars of religious edifices. In this study, we provide new archaeometric information on the raw materials, pigments and opacifying agents used to produce ―Marmi Mischi‖ of ―Pallium altaris‖ from the Messina Regional Museum. To reach this objective, all the studied glass decorations were analysed by means of non-destructive portable X-ray fluorescence (pXRF). Some of the decorations were further subjected to Environmental scanning electron microscopy (ESEM) and X-ray powder diffraction (XRPD) in the laboratory. Two types of glasses were recognised. The first one – bluish green in colour – is a basic or slightly modified ―carcara glass‖, characterized by high concentrations of P. The second type – dark blue, turquoise, light turquoise and red in colour – is a ―carcara glass‖ modified by craftsmen, containing high amounts of colouring agents (Cu, Pb, Sn, Sb). The presence of schreibersite in some of the analysed samples indicates that forming occurred in extremely reducing conditions and proves that the glasses were produced in CaO furnaces called ―carcara‖ and used to produce lime. Moreover, our results suggest that: i) the dark blue, turquoise and bluish green nuances are as a result of Fe2+, with minor contribution by Cu and Co; ii) the light turquoise nuance is related to Fe2+ and Cu2+, with minor contribution by Co; and iii) the red colour is as a result of the reduction of copper to the metallic state by Sn and Pb. Ca-antimonate (Ca2Sb2O7) was identified as an opacifying agent for the blue glassy decorations, whereas metallic Cu was identified for the red. The overall results of the chemical and physical characterization of the ―Pallium altaris‖ glassy decorations from the Messina Regional Museum suggest that the used raw material was ―carcara glass,‖ to which various chemical elements were suitably added to obtain the desired nuances.
    Description: Published
    Description: 97-111
    Description: 7SR AMBIENTE – Servizi e ricerca per la società
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2020-02-19
    Description: We constrained the origin and genetic environment of modern iron ooids (sand-sized grains with a core and external cortex of concentric laminae) providing new tools for the interpretation of their fossil counterparts as well as the analogous particles discovered on Mars. Here, we report an exceptional, unique finding of a still active deposit of submillimetric iron ooids, under formation at the seabed at a depth of 80 m over an area characterized by intense hydrothermal activity off Panarea, a volcanic island north of Sicily (Italy). An integrated analysis, carried out by X-ray Powder Diffraction, Environmental Scanning Electron Microscopy, X-ray Fluorescence and Raman spectroscopy reveals that Panarea ooids are deposited at the seafloor as concentric laminae of primary goethite around existing nuclei. The process is rapid, and driven by hydrothermal fluids as iron source. A sub-spherical, laminated structure resulted from constant agitation and by degassing of CO2-dominated fluids through seafloor sediments. Our investigations point the hydrothermal processes as responsible for the generation of the Panarea ooids, which are neither diagenetic nor reworked. The presence of ooids at the seawater-sediments interface, in fact, highlights how their development and growth is still ongoing. The proposed results show a new process responsible for ooids formation and gain a new insight into the genesis of iron ooids deposits that are distributed at global scale in both modern and past sediments.
    Description: Published
    Description: id 7107
    Description: 6A. Geochimica per l'ambiente e geologia medica
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    Publication Date: 2020-02-19
    Description: A variety of calcareous and siliceous skeletal components are associated with exceptional, still active deposits of modern iron ooids off Panarea, one of the volcanic islands of the Aeolian Arc (Tyrrhenian Sea, Italy). Both ooids and skeletal components occur as loose sediments influenced by submarine hydrothermal fluid vents. Whereas iron ooids are exclusively made of goethite laminae primarily nucleated on volcaniclastic material, sponge spicules – that represent most of the siliceous skeletal component – develop laminated coatings (concretions) of varying sizes. This partial or total coating consists of regularly banded Fe‒rich layers exhibiting the same textural features and mineralogical composition (goethite) of the ooid cortex developed around inorganic cores. Spicules did not reveal any obvious attaching structure or interfingering with the surrounding coating and did not undergo bioerosion or any other evidence of biological intervention during their development. A hydrothermal origin, compatible with the general setting, is therefore proposed for these armoured sponge spicules. We believe that this unique modern case of iron concretions produced on siliceous spicules can contribute to explain other known fossil cases as well as to understand the taphonomy of this type of biogenic silica that seems rarely to have been preserved in such an extreme habitat.
    Description: Published
    Description: 109379
    Description: 6A. Geochimica per l'ambiente e geologia medica
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 5
    Publication Date: 2020-03-23
    Description: The presence of heavy minerals, including radionuclides such as 238U and 232Th, in the beach placers outcropping along the western Calabrian coast (South Italy) has been investigated in order to single out the contribution from natural sources to the total radiation level. Assessing the human health radiation risk for these areas is of great importance due to their main touristic destination. With the aim of characterizing the natural radionuclides contents of the Calabrian sands, the correlations existing between their mineralogical and geochemical features and those of the parent rocks have been studied by measuring the sand radionuclides concentrations and decay products and by calculating the outdoor effective dose rate. The radioactivity in the Calabrian beach sediments is for the most part attributed to monazite and, in turn, to the high amount of Th (in the 409–464 ppm range), and is a function of the rock types and of the formation processes. The outdoor dose and effective dose rates for an exposure period of three months are in the range 1045–1240 nGy/h and 0.32–0.37 mSv/y, respectively. Although these values are remarkably higher than the corresponding average world values, they fall within the limits fixed by the Italian legislation, assuming individuals that spend three summer months on the beach. The results obtained for this area of the Southern Italy coastlines can be used as a baseline for future investigations concerning radioactivity background levels, also in other regions. Moreover, the coupling of the present findings with those of epidemiological studies will allow gaining a better evaluation of possible health effects on the population.
    Description: Published
    Description: P05015
    Description: 6A. Geochimica per l'ambiente e geologia medica
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 6
    Publication Date: 2019-03-27
    Description: This paper discusses the first geochemical characterization of obsidian fragments from the prehistoric site of Roccapalumba (Palermo, Italy). The Neolithic age of the prehistoric settlement was constrained by pottery and flint tools discovered in the same archaeological context. To define the provenance of the investigated obsidian artifacts major and trace element analyses have been carried out by using scanning electron microscopy (SEM–EDX) and inductively coupled plasma mass spectrometry (LA–ICP–MS). The comparison with literature data of the Central Mediterranean source areas, based on trace elements content and their ratios allow of constraining a provenance of the Roccapalumba obsidians from the Lipari Island. The obsidian lava flow from Gabellotto Valley is the most probable source of volcanic glass at Lipari and also the most exploited in the Mediterranean area for manufactured tools. The obtained results can contribute in reconstructing the trade/exchange and procurement relationships occurred between the prehistoric human groups inhabiting Sicily during Neolithic age.
    Description: Published
    Description: 151-167
    Description: 7SR AMBIENTE – Servizi e ricerca per la società
    Description: JCR Journal
    Keywords: Roccapalumba ; trace elements ; obsidian ; Neolithic ; SEM-EDX, ; Lipari Island ; LA-ICP-MS ; Archaeology and Archaeometry
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 7
    Publication Date: 2018-04-26
    Description: Petrological and geochemical data of Triassic magmatic rocks from Lercara Basin (Central Sicily), provide new information about the intraplate volcanism related to the Pangea break up. The magmatic rocks crop out as subvolcanic bodies and are packed in several Lower Triassic clayey lithologies correlated to the sedimentation inside the Imerese and Sicano domains. The samples are splitted in two groups: the first includes transitional to alkaline basalts, with sub-ophitic texture; the second includes more altered rocks, with porphyritic texture, showing alkali basaltic to phonolitic compositions. Major and trace element data of single groups show small variations indicating fractional crystallization processes. Abundances and ratios of incompatible trace elements indicate that rocks were formed in an intraplate continental environment from different mantle sources with E-MORB to OIB-type compositions. Low partial melting degrees at the transition between spinel and garnet lherzolite fields can be hypothesized for parental magmas of the Lercara Basin. We propose that magma batches moved toward the surface along lithospheric fractures originated by flexure and uplift of the Mesozoic Pangea supercontinent.
    Description: Published
    Description: 169-181
    Description: 2V. Struttura e sistema di alimentazione dei vulcani
    Description: JCR Journal
    Keywords: intraplate continental volcanism ; spinel-garnet-lherzolite source ; tectonic setting of triassic magmatism
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 8
    Publication Date: 2018-10-11
    Description: The results of a petrographic and geochemical study carried out on archeological grindstones allow to provide new constraints on protohistoric commercial exchanges over the Mediterranean area. Eleven grindstones, discovered in an archeological site located in Milazzo (Messina, Sicily) and dated from the Early Bronze Age, have been investigated by geochemical and petrographic techniques. The raw materials are mainly volcanic rocks characterized by calc-alkaline and K-alkaline affinities with volcanic arc geochemical signature. Only one sample, made of basalt belonging to the Naalkaline series, shows an intraplate signature. The comparison with the available literature data for similar rocks allowed constraining the volcanic origin of the exploited lavas. While the intraplate-type raw material came from Mt. Etna Volcano (Sicily), the arc-type volcanic rocks are mostly trachyandesites, basaltic andesites, and one rhyolite. Although most of them come from the Aeolian Arc, a provenance of some samples from the Aegean Arc cannot be excluded. This last region could represent the most probable provenance area for the rhyolite sample.
    Description: Published
    Description: 1571–1583
    Description: 6TM. Poli Museali
    Description: JCR Journal
    Keywords: Archeometry ; Volcanic rock ; Early Bronze Age ; SEM-EDS . XRF ; archeometric characterization
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 9
    Publication Date: 2019-03-26
    Description: The geological, biological and geochemical features of a particular field of hydrothermal vents, discovered in the Panarea Volcanic Complex during a research survey carried out in 2015, are described for the first time. The site, located at 70-80 m depth off the South-western coast of the islet of Basiluzzo, was named Smoking Land for the presence of a large number of wide and high active chimneys and was characterized in terms of dissolved benthic fluxes, associated macrofauna and megafauna communities and preliminary mineralogy and geochemistry of chimney structures. On the whole field, a total of 39 chimneys, different in size and shape, were closely observed and described; 14 of them showed emission of low temperature hydrothermal fluids of marine origin characterized by acidified chemical conditions. The CTD and benthic chamber measurements highlighted that the Smoking Land is able to form a sea water bottom layer characterized by variable acidity and high DIC and trace elements concentrations; these characteristics weaken moving away from the chimney mouths. The SEM-EDS analysis of the collected solid samples revealed a chimney structure principally composed by amorphous and low crystalline Fe-oxyhydroxides of hydrothermal origins. The ROV explorations revealed a wide coverage of red algae (Peyssonnelia spp.) colonized by the green algae Flabiella petiolata and by suspension feeders, mainly sponges, but also bryozoans, and tubicolous polychaetes. Although novent-exclusive species were identified, the benthic communities found in association to the chimneys included more taxa than those observed in the surrounding no-vent rocky areas. These first findings evidence a submarine dynamic habitat where geological, chemical and biological processes are intimately connected, making the Smoking Land an important site in terms of marine heritage that should be safeguarded and protected.
    Description: Published
    Description: 6A. Geochimica per l'ambiente e geologia medica
    Description: JCR Journal
    Keywords: hydrothermal fluids ; marine environment ; new shallow water hydrothermal vents over the Panarea volcanic area
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 10
    Publication Date: 2018-04-11
    Description: A well-preserved volcaniclastic sequence crops out in Pleistocene marine sediments along the Tyrrhenian coastline of the Calabrian-Peloritani arc (Sicily, Italy), testifying the occurrence of Lower-Middle Pleistocene volcanic activity in Southern Tyrrhenian Sea. The presence of dominant highly vesicular and minor blocky glassy particles indicates that the volcanic clasts were originated by explosive events related to the ascent and violent emission of volatile-rich magmas accompanied by and/or alternated with hydromagmatic fragmentation due to magma-sea water interaction. Field investigations and sedimentological features of the studied volcaniclastic units suggest a deposition from sediment-water density 􀃀ows. The chemical classi􀂿cation of the pumice clasts indicates prevalent rhyolitic and dacitic compositions with calc-alkaline to high-K calc-alkaline af􀂿nity. The geochemical features of immobile trace elements together with the presence of orthopyroxene are indicative of a provenance from an arc-type environment. The age (from 980-910 to 589 ka), the chemical composition and the evidence of subaerial explosive volcanic activity constrain the origin nature and temporal evolution of the arc-type volcanism in the Southern Tyrrhenian domain. Finally, the new information here provided contribute to a better understanding of the temporal geodynamic evolution of this sector of the Mediterranean domain.
    Description: Published
    Description: 371-389
    Description: 1V. Storia eruttiva
    Description: JCR Journal
    Keywords: volcaniclastic deposits ; Pleistocene volcanism ; new evidence for calc-alkaline explosive volcanism in the Southern Tyrrhenian Sea
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...